2019
DOI: 10.1029/2019wr024919
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Mechanisms, Upscaling, and Prediction of Anomalous Dispersion in Heterogeneous Porous Media

Abstract: We study the upscaling and prediction of large‐scale solute dispersion in heterogeneous porous media with focus on preasymptotic or anomalous features such as tailing in breakthrough curves and spatial concentration profiles as well as nonlinear evolution of the spatial variance of the concentration distribution. Spatial heterogeneity in the hydraulic medium properties is represented in a stochastic modeling approach. Direct numerical Monte Carlo simulations of flow and advective particle motion combined with … Show more

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Cited by 39 publications
(64 citation statements)
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“…The convergence toward a steady‐state velocity PDF shows the ergodic property of the underlying flow field. Note that ergodicity can be recovered even in purely advective flows as particles sample heterogeneous velocities along the trajectories in ergodic velocity fields (Comolli et al., 2019; Puyguiraud et al., 2019).…”
Section: Simulation Results and Analysismentioning
confidence: 99%
“…The convergence toward a steady‐state velocity PDF shows the ergodic property of the underlying flow field. Note that ergodicity can be recovered even in purely advective flows as particles sample heterogeneous velocities along the trajectories in ergodic velocity fields (Comolli et al., 2019; Puyguiraud et al., 2019).…”
Section: Simulation Results and Analysismentioning
confidence: 99%
“…Some of these assumptions may be relaxed in future studies to deal with realistic, heterogeneous formation with an autocorrelated permeability field. For that purpose, other approaches such as stochastic modeling and/or numerical modeling, rather than the deterministic analytical modeling of this study, are probably more suitable (Comolli et al, 2019; Di Dato et al, 2019; Fiori et al, 2017).…”
Section: Discussionmentioning
confidence: 99%
“…Thus, advective particle motion is quantified by the following stochastic evolution equations for the longitudinal particle position x(s) and the advective travel time t a (s) (Dentz et al, 2016;Comolli et al, 2019):…”
Section: Upscaled Transport Modelmentioning
confidence: 99%
“…The distance s along the streamline is in general larger than the linear travel distance x in the mean flow direction. They are projected onto each other through the advective tortuosity χ , which is given by the ratio of the average flow speed ⟨ q ⟩ and the average velocity component ⟨ q 1 ⟩ in mean flow direction, χ=qfalse/q1 (Comolli et al., 2019). The angular brackets denote suitably chosen averages, here spatial and ensemble average.…”
Section: Upscaled Transport Modelmentioning
confidence: 99%
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